These synthetic motions are usually desired to be spatially correlated, site reflected, nonstationary, and compatible with target design response spectra.
This value shows that the recognition rates per style for original motions versus synthetic motions are tightly linked.
The values of all style recognition rates for both original and synthetic motions are presented in Figure 6.
It is preferable to use simpler fault geometry to predict strong ground motions for future earthquakes if synthetic motions that fit the observed motions reasonably well can be obtained.
The synthetic motions obtained with the EGF method agree with the observed motions with respect to acceleration, velocity, and displacement in the frequency range from 0.3 to 10 Hz.
For example, RG 1.208 explicitly prohibits the use of synthetic motions that are not based on seed-recorded time histories so that only modified recorded ground motions can be used for site response analysis.
By cutting down the possible paths, according to the input audio, we reduce the ambiguity of the mapping from audio to visual speech movements and produce more realistic synthetic motions.
A source model for generating strong ground motions during the 2011 off the Pacific coast of Tohoku Earthquake (Mw 9.0) is estimated from a comparison of the observed records of the mainshock and synthetic motions, based on the characterized source model using the empirical Green's function method.
The synthetic motions agree with the observed motions for acceleration, velocity, and displacement, as shown in Fig. 10, including at KMMH16 (KiK-net Mashiki), KMMH14 (KiK-net Toyono) and KMM005 (K-NET Ohzu), which are located very near the source fault.
The locations and areas of the SMGAs were determined through comparison between the synthetic ground motions and observed motions.
